• Bulletin of the Korean Space Science Society
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• 2010.04a
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• pp.40.1-40.1
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• 2010

한국천문연구원 우주과학연구본부 태양우주환경연구그룹은 일본 Tierra Tecnica사의 RFP-523C Overhauser Proton 자력계와 MISYS-09 삼축 MI 자력계를 2009년 11월에 보현산천문대 태양망원경동에 구축하였다. 한국천문연구원은 이미 2007년 11월에 RFP-523C Fluxgate 자력계를 보현산천문대 태양망원경동에 구축하여 K 지수 산출 등의 우주환경예 경보 연구에 활용하고 있다. Fluxgate 자력계는 지자기 3축 성분의 변화량을 측정하는 장비이고 이번에 설치한 Overhauser Proton 자력계는 지자기의 총 자기장을 측정하는 장비이다. 삼축 MI 자력계는 지자기장의wave를 측정하는 장비이다. 기존에 설치한 Fluxgate 자력계와 새로 설치한 Proton 자력계, 삼축 MI 자력계를 연계하여 운용할 경우 우주환경에 의한 지자기장 변화량의 측정 정밀도가 향상되고 지자기장을 효율적으로 관측할 수 있다. 보현산천문대에 구축한 각각의 자력계가 측정한 지자기 자료들은 S-FTP와 Socket 통신을 이용하여 대전에 있는 한국천문연구원 태양우주환경연구그룹의 데이터 서버로 실시간으로 전송되어 저장되고 있다. 데이터 서버로 전송된 지자기 측정 자료들은 한국천문연구원 우주환경감시실에서 모니터링하고 있다.

• Journal of Sensor Science and Technology
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• v.5 no.4
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• pp.9-15
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• 1996

In order to display magnetic signals obtained from a magneto-resistance sensor, a direct current magnetometer was designed and its circuit was constructed. The magnetic fields measured by the home-made magnetometer, which showed good functions of automatic ranging, analog output, and vector sensing, were well agreed with those by commercial MAG-01 magnetometer. The measurement range of the magnetometer was $1\;{\mu}T$ to 1.999 mT, the resolution was -132 dB within 1 Hz bandwidth and the measured magnetic fields could be displayed with $3{\cdot}1/2$-digit LED.

• Journal of Astronomy and Space Sciences
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• v.19 no.4
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• pp.293-304
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• 2002

This paper describes the re-design and the calibration results of the MAG digital circuit onboard the KSR-3. We enhanced the sampling rate of magnetometer data. Also, we reduced noise and increased authoritativeness of data. We could confirm that AIM resolution was decreased less than InT of analog calibration by a digital calibration of magnetometer. Therefore, we used numerical-program to correct this problem. As a result, we could calculate correction and error of data. These corrections will be applied to magnetometer data after the launch of KSR-3.

• Journal of Astronomy and Space Sciences
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• v.14 no.2
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• pp.312-319
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• 1997

The magnetometer is one of the most important payloads for scientific satellite to monitor the near-earth space environment. The electromagnetic variations of the space environment can be observed with the electric and magnetic field measurements. In practice, it is well known that the measurement of magnetic fields needs less technical complexities than that of electric fields in space. Therefore the magnetometer has long been recognized as one of the basic payloads for the scientific satellites. In this paper, we discuss the scientific fluxgate magnetometer which will be on board the KITSAT-3. The main circuit design of the present magnetometer is based on that of KITSAT-1 and -2 but its facilities have been re-designed to improve the resolution to about 5nT for scientific purpose. The calibration and noise level test of this circuit have been performed at the laboratory of the Tierra Tecnica company in Japan.

• Geophysics and Geophysical Exploration
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• v.27 no.2
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• pp.119-128
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• 2024

Marine magnetic surveys provide a rapid and cost-effective method for pioneer geophysical survey for many purposes. Sea-surface magnetometers offer high accuracy but are limited to measuring the scalar total magnetic field and require dedicated cruise missions. Shipboard three-component magnetometers, on the other hand, can collect vector three components and applicable to any cruise missions. However, correcting for the ship's magnetic field, particularly viscous magnetization, still remains a challenge. This study proposes a new additional correction method for ship's viscous magnetization effect in vector data acquired by shipboard three-component magnetometer. This method utilizes magnetic data collected simultaneously with a sea-surface magnetometer providing total magnetic field measurements. Our method significantly reduces deviations between the two datasets, resulting in corrected vector anomalies with errors as low as 7-25 nT. These tiny errors are possibly caused by the vector magnetic anomaly and its related viscous magnetization. This method is expected to significantly improve the accuracy of shipborne magnetic surveys by providing corrected vector components. This will enhance magnetic interpretations and might be useful for understanding plate tectonics, geological structures, hydrothermal deposits, and more.

• 한국지구과학회:학술대회논문집
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• 2010.04a
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• pp.124-127
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• 2010

본 연구에서는 통가 해역 라우분지의 열수 광상 가능성이 있는 해산들에 대하여 자력탐사가 수행되었다. 그 중 TA 09 해산에 대하여 심해견인 자력탐사가 실시되었으며 심해견인 자력탐사는 정밀한 탐사를 위하여 해저면에서 약 50 ~ 60 m 고도를 유지하며 자력계를 견인하였다. 탐사지역의 총 자력 성분은 Overhauser Proton Magnetomer (모델 SeaSPY 300(해상자력계)m, SeaSPY 6000(심해견인자력계))를 이용하여 측정되었다. 탐사 해산들 중 해상자력탐사와 심해자력탐사가 같이 수행된 TA 09 해산과 주요 열수 광상 유망 지역으로 분류되는 TA 12, 26 해산에 대해서만 측정된 지자기값을 이용하여 자기이상도를 구하였으며 자화역산법을 이용하여 자화이상도를 제작하고 분석하였다. TA 09 해산과 TA 26 해산에서의 해상 자기이상도는 쌍극자 이상형태의 단순이상을 보이며 TA 12 해산에서는 정상부에 고이상이 나타나고 그 주변으로는 저이상대가 분포하고 있다. TA 09 해산에서의 해상자력계에 의한 자기이상치와 심해견인자력계에 의한 자기이상치를 비교하여 보면 거의 10배 이상의 해상도 차이를 보여준다. 연구지역 탐사해산들의 해저지형과 비교하여 보면 열수분출대의 가능성이 높은 저자화이상대들은 주로 해산의 정상부 및 정상부 칼데라와 그 칼데라 주변부에 주로 위치하고 있는 모습을 나타내고 있다. 향후 타 탐사 해산들에 대한 자기이상에 대한 정밀처리/분석 후 탄성파 탐사결과, 암석샘플의 결과 및 지화학결과 등과 비교하여 열수광상의 존재 여부 및 위치 추정 분석이 필요할 것으로 판단된다.

• Journal of the Korea Institute of Information and Communication Engineering
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• v.18 no.12
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• pp.3069-3078
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• 2014

This research handles the performance improvement effect by the Modeling & Simulation and shows the design, implementation, test results of the new 3-axis magnetometer which is the core component of strategic offensive deploying mine. The submarine is modelled by using the commercial electromagnetic field analysis tool on numerical value, and its magnetic field characteristic is predicted in order to apply the new magnetometer to the future underwater weapon system. The method to take the performance test results of new 3-axis magnetometer in the land is shown instead of the real test result in sea by making the miniature submarine.

• Bulletin of the Korean Space Science Society
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• 2003.10a
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• pp.71-71
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• 2003

과학로켓 3호에 탑재된 자력계의 데이터 분석을 통해서 로켓의 비행자세가 어떻게 비행시간에 따라 어떻게 변화했는지에 대해 논한다. 과학로켓 3호에 탑재된 로켓의 비행 자세 정보 획득을 위한 Fluxgate 자력계인 Attitude Information Magnetometer (AM)의 데이터 분석을 통해 로켓의 비행시간동안 자세가 어떻게 변화했는지 수치해석 프로그램 및 시뮬레이션을 통해 알아보았다 본 연구에서 사용한 수치해석 프로그램은 Spline 보정법, 다항식 수치법인 Bairstow Method, Least square method이며, 자체 개발한 로켓비행정보 획득용 프로그램과 OpenGL을 이용한 로켓의 3차원 시뮬레이션을 통해서 과학로켓 3호의 자세를 나타내는 roll, pitch, yaw의 변화를 알아보았다. 그리고, 이 결과를 이용하여 자력계가 자세제어에 적합한지도 분석하였다.

• Journal of Biomedical Engineering Research
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• v.24 no.3
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• pp.159-165
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• 2003

We developed a 37-channel magnetoencephalogram (MEG) measurement system based on low-noise superconducting quantum interference device (SQUID) magnetometets, and operated the system to measure MEG signals. By using double relaxation oscillation SQUIDs with high flux-4o-voltage transfers, the SQUID outputs could be measured directly by room temperature preamplifiers and compact readout circuits were used for SQUID operation. The average field noise level of the magnetometers is about 3 fT/√Hz in the white region, low enough for MEG measurements when operated inside a magnetically shielded room. The 37 magnetometers were distributed on a hemispherical surface haying a radius of 125 mm. In addition to the 37 sensing channels. 11 reference channels were installed to pickup external noise and to form software gradiometers. A low-noise liquid helium dewar was fabricated with a liquid capacity of 30 L and boil-off rate of 4 L/d. The signal processing software consists of digital filtering, software gradiometer, isofield mapping and source localization. By using the developed system, we measured auditory-evoked fields and localized the current dipoles, demonstrating the effectiveness of the system.

• Geophysics and Geophysical Exploration
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• v.23 no.2
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• pp.67-71
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• 2020

In this study, we derive closed-form expressions of magnetic gradient tensor due to a circular cylinder. Because the expression for magnetic field has been derived in a previously conducted study, expressions are developed for the magnetic gradient tensor based on the derivatives of the expressions of magnetic field with respect to the variables of the Cartesian coordinates. Furthermore, expressions are derived for the magnetic gradient tensor based on the relations between the Cartesian and cylindrical coordinates in the derivative because the expression for magnetic field contains variables of cylindrical coordinates owing to its axial symmetry.